地埋点源滴灌土壤水分运动规律的研究

    Research for Soil Water Movement From a Buried Trickle Source

    • 摘要: 根据非饱和土壤水运动理论,建立了地埋点源滴灌条件下土壤水分运动的数学模型,针对地埋点源入渗的特点,采用了可动的边界条件,加快了有限差分法对模型求解速度。应用模型分析了地埋点源滴灌土壤水分运动的基本规律,由此对地埋点源滴灌系统的设计和运行管理提出了初步看法

       

      Abstract: A Mathematicalmodel was developed to simulate soil water infiltration from a buried trickle source. The model was solved numerically by an approach of the noniterative ADI difference procedure. And variable boundaries were used for saving computing time. The numerical results were compared with field test. The comparisons indicated that the method is reliable. Typical results showed the effect of trickle discharge, irrigation volume and buried depth of dripper on soil moisture content and the wetted pattern. Some suggestions were presented by the numerical results for design and management of sub-surface trickle irrigation.

       

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